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Stable isotopic ratios of hydrogen and oxygen in groundwater and calculated fraction of recharge from winter precipitation, South Rim Grand Canyon, Arizona

Dates

Publication Date
Start Date
1992-09-01
End Date
2019-05-09

Citation

Solder, J.E., 2020, Stable isotopic ratios of hydrogen and oxygen in groundwater and calculated fraction of recharge from winter precipitation, South Rim Grand Canyon, Arizona: U.S. Geological Survey data release, https://doi.org/10.5066/P9G7INFB.

Summary

Dataset provides inputs and model results of a stable isotope-based mixing model for estimating the relative contribution of seasonal recharge sources to the South Rim groundwater flow system, Grand Canyon, Arizona, USA.

Contacts

Point of Contact :
John E Solder
Originator :
John E Solder
Metadata Contact :
John E Solder
Publisher :
U.S. Geological Survey
Distributor :
U.S. Geological Survey - ScienceBase
SDC Data Owner :
Utah Water Science Center
USGS Mission Area :
Water Resources

Attached Files

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StableIso_Metadata.xml
Original FGDC Metadata

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18.65 KB application/fgdc+xml
Table1_GroundwaterData_CalculatedFractionWinter.xlsx 43.87 KB application/vnd.openxmlformats-officedocument.spreadsheetml.sheet

Purpose

Groundwater data was collected and compiled from published literature to evaluate the source and flow paths of groundwater. Stable isotopic ratios of hydrogen and oxygen in water were used to evaluate the seasonal precipitation source of groundwater recharge. The mixing model is described in Solder and Beisner (2020), which estimates mixing end-members from precipitation and surface water data. The final calculated value is the fraction of recharge from winter precipitation as reported here. Solder, J.E., and Beisner, K.R., 2020, Critical evaluation of stable isotope mixing end-members for estimating groundwater recharge sources: case study from the South Rim of the Grand Canyon, Arizona, USA, Hydrogeology Journal

Additional Information

Identifiers

Type Scheme Key
DOI https://www.sciencebase.gov/vocab/category/item/identifier doi:10.5066/P9G7INFB

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